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Abundance, activity and community structure of denitrifiers in drainage ditches, in relation to sediment characteristics, vegetation and land-use

机译:排水沟中反硝化器的丰度,活性和群落结构与沉积物特征,植被和土地利用的关系

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摘要

Drainage ditches are ubiquitous yet understudied features of the agricultural landscape. Nitrogen pollution disrupts the nutrient balance of drainage ditch ecosystems, as well as the waterbodies in which they drain. Denitrification can help ameliorate the impact of N-fertilization by converting reactive nitrogen into dinitrogen gas. However, factors affecting denitrification in drainage ditches are still poorly understood. In this study, we tested how within-ditch and regional environmental conditions affect denitrifier activity, abundance, and community structure, to understand controls on denitrification at multiple scales. To this end, we quantified in situ denitrification rates and denitrifier abundance in 13 drainage ditches characterized by different types of sediment, vegetation and land-use. We determined how denitrification rates relate to denitrifier abundance and community structure, using the presence of nirS, nirK and nosZ genes as a proxy. Denitrification rates varied widely between the ditches, ranging from 0.006 to 24 mmol N m−2 h−1. Ditches covered by duckweed, which contained high nitrate concentrations and had fine, sandy sediments, were denitrification hotspots. We found highest rates in ditches next to arable land, followed by those in grasslands; lowest rates were observed in peatlands and nature reserves. Denitrification correlated to nitrate concentrations, but not to nirK, nirS and nosZ abundance, whereas denitrifier-gene abundance correlated to organic matter content of the sediment, but not to nitrate concentrations. Our results show a mismatch in denitrification regulators at its different organizational scales. Denitrifier abundance is mostly regulated at within-ditch scales, whereas N-loads, regulated by landscape factors, are most important determinants of instantaneous denitrification rates.
机译:排水沟是农业景观普遍存在但尚未被研究的特征。氮污染破坏排水沟生态系统以及排水沟生态系统的养分平衡。反硝化可以通过将反应性氮转化为氮气来帮助缓解氮肥的影响。然而,影响排水沟反硝化的因素仍然知之甚少。在这项研究中,我们测试了沟内和区域环境条件如何影响反硝化器的活动,丰度和群落结构,以了解多种规模的反硝化控制。为此,我们定量分析了以沉积物,植被和土地利用的不同类型为特征的13个排水沟的原位反硝化率和反硝化能力。我们使用nirS,nirK和nosZ基因作为替代物,确定了反硝化率与反硝化菌丰度和群落结构的关系。沟渠之间的反硝化率差异很大,范围为0.006至24 mmol N m-2 h-1。浮萍覆盖的沟渠是反硝化的热点,该沟渠中的硝酸盐浓度很高,并且沉积物细腻,沙状。我们发现,耕地旁的沟渠率最高,其次是草原。泥炭地和自然保护区的比率最低。反硝化作用与硝酸盐浓度相关,但与nirK,nirS和nosZ的丰度无关,而反硝化剂基因的丰度与沉积物的有机质含量有关,但与硝酸盐浓度无关。我们的结果表明,不同组织规模的反硝化调节剂不匹配。反硝化剂的丰度主要在沟内尺度上调节,而氮负荷(受景观因素调节)是瞬时反硝化速率的最重要决定因素。

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